Functional waters in intraprotein proton transfer monitored by FTIR difference spectroscopy.

Much progress has been made in our understanding of water molecule reactions on surfaces, proton solvation in gas-phase water clusters and proton transfer through liquids. Compared with our advanced understanding of these physico-chemical systems, much less is known about individual water molecules and their cooperative behaviour in heterogeneous proteins during enzymatic reactions. Here we use time-resolved Fourier transform infrared spectroscopy (trFTIR) and in situ H2(18)O/H2(16)O exchange FTIR to determine how the membrane protein bacteriorhodopsin uses the interplay among strongly hydrogen-bonded water molecules, a water molecule with a dangling hydroxyl group and a protonated water cluster to transfer protons. The precise arrangement of water molecules in the protein matrix results in a controlled Grotthuss proton transfer, in contrast to the random proton migration that occurs in liquid water. Our findings support the emerging paradigm that intraprotein water molecules are as essential for biological functions as amino acids.

Molecular architecture and conformational flexibility of human RNA polymerase II.

Transcription by RNA polymerase II (RNAPII) is a central process in eukaryotic gene regulation. While atomic details exist for the yeast RNAPII, characterization of the human complex lags behind, mostly due to the inability to obtain large quantities of purified material. Although the complexes have the same protein composition and high sequence similarity, understanding of transcription and of transcription-coupled DNA repair (TCR) in humans will require the use of human proteins in structural studies. We have used cryo-electron microscopy, image reconstruction, and variance analysis to characterize the structure and dynamics of human RNAPII (hRNAPII). Our studies show that hRNAPII in solution parallels the conformational flexibility of the yeast structures crystallized in different states but also illustrate a more extensive conformational range with potential biological significance. This hRNAPII study will serve as a structural platform to build up higher-order transcription and TCR complexes and to gain information that may be unique to the human RNAPII system.

Octomeric pyruvate-ferredoxin oxidoreductase from Desulfovibrio vulgaris.

Pyruvate-ferredoxin oxidoreductatse (PFOR) carries out the central step in oxidative decarboxylation of pyruvate to acetyl-CoA. We have purified this enzyme from Desulfovibrio vulgaris Hildenborough (DvH) as part of a systematic characterization of as many multiprotein complexes as possible for this organism, and the three-dimensional structure of this enzyme has been determined by a combination of electron microscopy (EM), single particle image analysis, homology modeling and computational molecular docking. Our results show that the 1MDa DvH PFOR complex is a homo-octomer, or more precisely, a tetramer of the dimeric form of the related enzyme found in Desulfovibrio africanus (Da), with which it shares a sequence identity of 69%. Our homology model of the DvH PFOR dimer is based on the Da PFOR X-ray structure. Docking of this model into our 17A resolution EM-reconstruction of negatively stained DvH PFOR octomers strongly suggests that the difference in oligomerization state for the two species is due to the insertion of a single valine residue (Val383) within a surface loop of the DvH enzyme. This study demonstrates that the strategy of intermediate resolution EM reconstruction coupled to homology modeling and docking can be powerful enough to infer the functionality of single amino acid residues.

Polarized FTIR spectroscopy in conjunction with in situ H/D exchange reveals the orientation of protein internal carboxylic acids.

Polarized Fourier transform infrared (FTIR) difference spectroscopy has been combined with in situ H/D exchange measurements to investigate the orientation of single protonated carboxylic acids within bacteriorhodopsin (bR), exclusively based on the protein ground state. The combination of these two techniques enables the determination of the C=O dipole moment direction of D115 and D96 relative to the membrane plane to 68 +/- 11 and 45 +/- 4 degrees , respectively. By discussing these results in the context of X-ray structure analysis, we are able to determine which of the two oxygen atoms of the respective carboxylic acids binds the proton. In the case of D115, it is the oxygen which is located close to T90. On the basis of this finding, we show a possible interaction path between D115 and D85, which has been proposed to be responsible for the inhibition of the proton pump efficiency to prevent over-acidification of the external medium known as the back-pressure effect. Because the orientation of carboxylic acids can be determined even when the group does not undergo any protonation changes during the photocycle, as shown in the case of D115, the method can be applied to any orientable protein and is not merely restricted to bR.

A time-resolved iron-specific X-ray absorption experiment yields no evidence for an Fe2+ --> Fe3+ transition during QA- --> QB electron transfer in the photosynthetic reaction center.

Previous time-resolved FTIR measurements suggested the involvement of an intermediary component in the electron transfer step Q(A)- --> Q(B) in the photosynthetic reaction center (RC) from Rhodobacter sphaeroides [Remy and Gerwert (2003) Nat. Struct. Biol. 10, 637]. By a kinetic X-ray absorption experiment at the Fe K-edge we investigated whether oxidation occurs at the ferric non-heme iron located between the two quinones. In isolated reaction centers with a high content of functional Q(B), at a time resolution of 30 micros and at room temperature, no evidence for transient oxidation of Fe was obtained. However, small X-ray transients occurred, in a similar micro- to millisecond time range as in the IR experiments, which may point to changes in the Fe ligand environment due to the charges on Q(A)- and Q(B)-. In addition, VIS measurements agree with the IR data and do not exclude an intermediate in the Q(A)- --> Q(B) transition.

Proton binding within a membrane protein by a protonated water cluster.

Proton transfer is crucial for many enzyme reactions. Here, we show that in addition to protonatable amino acid side chains, water networks could constitute proton-binding sites in proteins. A broad IR continuum absorbance change during the proton pumping photocycle of bacteriorhodopsin (bR) indicates most likely deprotonation of a protonated water cluster at the proton release site close to the surface. We investigate the influence of several mutations on the proton release network and the continuum change, to gain information about the location and extent of the protonated water network and to reveal the participating residues necessary for its stabilization. We identify a protonated water cluster consisting in total of one proton and about five water molecules surrounded by six side chains and three backbone groups (Tyr-57, Arg-82, Tyr-83, Glu-204, Glu-194, Ser-193, Pro-77, Tyr-79, and Thr-205). The observed perturbation of proton release by many single-residue mutations is now explained by the influence of numerous side chains on the protonated H bonded network. In situ hydrogen/deuterium exchange Fourier transform IR measurements of the bR ground state, show that the proton of the release group becomes localized on Glu-204 and Asp-204 in the ground state of the mutants E194D and E204D, respectively, even though it is delocalized in the ground state of wild-type bR. Thus, the release mechanism switches between the wild-type and mutated proteins from a delocalized to a localized proton-binding site.

The assignment of the different infrared continuum absorbance changes observed in the 3000-1800-cm(-1) region during the bacteriorhodopsin photocycle.

The bleach continuum in the 1900-1800-cm(-1) region was reported during the photocycle of bacteriorhodopsin (bR) and was assigned to the dissociation of a polarizable proton chain during the proton release step. More recently, a broad band pass filter was used and additional infrared continua have been reported: a bleach at >2700 cm(-1), a bleach in the 2500-2150-cm(-1) region, and an absorptive behavior in the 2100-1800-cm(-1) region. To fully understand the importance of the hydrogen-bonded chains in the mechanism of the proton transport in bR, a detailed study is carried out here. Comparisons are made between the time-resolved Fourier transform infrared spectroscopy experiments on wild-type bR and its E204Q mutant (which has no early proton release), and between the changes in the continua observed in thermally or photothermally heated water (using visible light-absorbing dye) and those observed during the photocycle. The results strongly suggest that, except for the weak bleach in the 1900-1800-cm(-1) region and >2500 cm(-1), there are other infrared continua observed during the bR photocycle, which are inseparable from the changes in the absorption of the solvent water molecules that are photothermally excited via the nonradiative relaxation of the photoexcited retinal chromophore. A possible structure of the hydrogen-bonded system, giving rise to the observed bleach in the 1900-1800-cm(-1) region and the role of the polarizable proton in the proton transport is discussed.